Results 61 to 70 of about 1,338 (112)
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Tillites et tilloïdes du massif armoricain

Palaeogeography, Palaeoclimatology, Palaeoecology, 1985
Abstract A glacial origin had been suggested for the Upper Brioverian pebble mudstones of the Armorican Massif. The lack of any true evidence of glacial abrasion on the pebbles, the turbiditic sedimentary environment and the great amount of resedimentation figures would rather plead for a deposition by debris-flow or mass-flow.
Dore, Francis, Dupret, L., Le Gall, J.
openaire   +2 more sources

Un aperçu de la métallogénie du Massif armoricain : Les minéralisations antimonifères du Massif armoricain

2016
National ...
Pochon, Anthony   +4 more
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Upper Proterozoic Basaltic Volcanism in the Northern Massif Armoricain, France

Geological Society, London, Special Publications, 1987
Summary A 2 km thick sequence of subaqueous basaltic rocks—the Hillion-Erquy Volcanic Formation (HEVF)—forms the lower part of the late Proterozoic Brioverian supracrustal sequence around the Baie de St. Brieuc, N Brittany. Basic dykes cutting the adjacent Pre-Brioverian crystalline basement (the Pentevrian) are interpreted as feeders to the ...
G. J. Lees   +3 more
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Le Mio-Pliocène du Massif armoricain. Données nouvelles

Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science, 1998
Abstract The ‘red sands’ of the Armorican Massive were attributed to an upper Pliocene marine environment. A reappraisal of the stratigraphy and ESR datings shows that it covers fluviatile to estuarine retrogressive formations, invading paleovalleys, and covering Tortonian, Messinian, Zanclean and Lower Piacenzian high stands.
Brigitte Van Vliet-Lanoë   +8 more
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Les Ptéridophytes du Massif Armoricain, passé et perspectives

Bulletin de la Société Botanique de France. Lettres Botaniques, 1986
ResumeListe des especes et hybrides de Pteridophytes observes dans le Massif Armoricain. Pour chaque espece, un commentaire donne des indications ecologiques sommaires, l'evolution de la repartition depuis le siecle dernier ainsi que l'etat de nos connaissances sur la repartition actuelle.
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